Unit 6 Flashcards

(33 cards)

1
Q

Streak

A

Mark left behind from a mineral
Rub against streak plate to determine streak
⭐️color of mineral may change but streak color doesn’t⭐️

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2
Q

Luster

A

Shine: metallic

No shine: non metallic, dull, glassy(reflective)

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3
Q

Breakage pattern

A

Cleavage: minerals tendency to break into pattern
Fracture: break randomly, uneven

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4
Q

Cleavage

A

Thin sheets, one direction
Cubic, 90 angle
Rhombohedral, slanted cube

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5
Q

Hardness

A

Resistance to being scratched
Scale of 1-10
Test on glass plate

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6
Q

Glass test

A

See if scratched or scratches
Scratches glass: 5.5<
No scratch on glass: 5.5>

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7
Q

Density

A

Mass/ volume

Can use to compare minerals

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8
Q

What are rocks and types

A

Made up of minerals, are solids

Igneous, sedimentary, metamorphic

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9
Q

Igneous rocks forming

A

Molten rocks —> solidified

Hardening of melted rocks/ molten rocks

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10
Q

Origin

A

Location of where molten rock solidifies. Intrusive and extrusive.

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11
Q

Intrusive

A

Inside volcano

Large crystals

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12
Q

Extrusive

A

Outside volcano

Small crystals

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13
Q

Texture

A

Size, shape of mineral in/on rock

Fine grain, vesicular, coarse grained, glassy

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14
Q

Fine grained

A
Fast cooling
small crystals(can’t grow, not enough time)
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15
Q

Vesicular

A
Fast cooling 
tiny holes(gas escape) vesicles
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16
Q

Coarse grained

A
Individual large crystals 
Slow cooling(time to grow)
17
Q

Glassy

A

Fast(est) cooling

No mineral growth

18
Q

Mineral composition

A

Silica content of minerals
proportions of light and dark
Felsic and mafic

19
Q

Silica

A

Material formed from oxygen and silicon

20
Q

Felsic

A

SiO(2)Al
Light colored
From thick and slow flowing magma
Low density

21
Q

Mafic

A

FeMg
Dark colored
Hot and thin fluid magma
High density

22
Q

Silicates

A

Si and O
Most common group of minerals
Most abundant elements in earths crust

23
Q

Non silicate

A

Do not contain BOTH Si and O

24
Q

Silicon-oxygen tetrahedron

A

Si in middle 4 O surrounding it in Diamond form

25
Pg 16
Minerals properties
26
Pg 6
Igneous rock identification How to use chart: 1) draw straight line/make sure a line is present 2) take paper, set to scale and copy scale 3) put 0% to straight line and bottom line of where it intersects with given mineral 4) count the ticks until you reach top line of mineral 5) the tick at top line is the percent of mineral found in the rock
27
Bowen series
``` Created by N.L. Bowen in 1900s Determines when/at what temp minerals crystallize at. Orderly sequence Discontinuous and continuous High temp of crystallization = mafic Low temp of crystallization = felsic ```
28
Discontinuous
Different minerals formed Olivine forms first in hottest magma as it cools —> pyroxene and so on
29
Continuous
Same mineral | plagioclase goes from all Ca —> all Na as temp goes from hot —> cool
30
Potassium feldspar—> quartz
Last to form as magma cools temp decreases
31
What is a mineral
``` Makes up most of rocks Grow to crystals when reach full growth potential -Naturally occurring -inorganic solid -definite chemical composition -crystal(atomic) structure ```
32
Chemical composition
Made from chemical elements | Expressed in chem. formula
33
Crystal structure
Formed from elements Specific pattern of atoms Mineral shape reflects atoms arrangement